Observed Seismicity - University of Kentucky
Observed Seismicity - University of Kentucky
Observed Seismicity - University of Kentucky
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Discussion<br />
9<br />
Figure 9. Seismic recordings <strong>of</strong> the Bardwell event from station BLKY.<br />
Table 4. Comparison <strong>of</strong> parameters <strong>of</strong> the Bardwell, Ky., and Blytheville, Ark., earthquakes.<br />
Date Time Magnitude Location Focal Depth<br />
(EDT) (M w<br />
) (La./Lo.) (km)<br />
06/06/2003 8:29:34 a.m. 4.0 36.88N/88.98W 2.3<br />
04/30/2003 0:56:22 a.m. 4.0 35.92N/89.92W 23.8<br />
The observed seismicity between January<br />
and June 2003 in the New Madrid Seismic<br />
Zone indicates that (1) most recorded<br />
seismicity in the central United States reflects<br />
the active faults <strong>of</strong> the New Madrid Seismic<br />
Zone and (2) in the Jackson Purchase Region,<br />
characteristics <strong>of</strong> earthquakes, such as focal<br />
depth, are different from those <strong>of</strong> earthquakes<br />
in the central New Madrid Seismic<br />
Zone. Six months <strong>of</strong> seismic monitoring is<br />
not enough time to make a scientifically<br />
defensible conclusion about the extent <strong>of</strong> the<br />
active faults into the Jackson Purchase Region.<br />
Much more time is needed for seismic<br />
monitoring in the area. The observed seismicity<br />
suggests, however, that the active<br />
faults <strong>of</strong> the New Madrid Seismic Zone may<br />
not extend into the Jackson Purchase Region.<br />
This could result in lower estimates <strong>of</strong> the<br />
seismic hazard in western <strong>Kentucky</strong>.